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Regional difference in the characteristics of dust event in East Asia

机译:东亚沙尘事件特征的区域差异

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The regional difference in the characteristics of dust event in East Asia was investigated by use of surface meteorological data from March 1988 to May 2004. Referring to the topography and land cover type, East Asia was divided into 11 regions. Among these regions, dust outbreaks frequently occur in Gobi Desert, the western part of Loess Plateau, and Taklimakan Desert whose land cover types are Bare Desert and Semi Desert Shrubs (i.e., desert). Although the result of frequent dust outbreaks is common among these regions, the frequency of floating dusts differs greatly. Floating dusts are frequently observed in Taklimakan Desert. On the other hand, floating dusts are seldom observed in Gobi Desert and Loess Plateau. In these regions, although dusts are produced by synoptic disturbances, they are immediately swept away by these synoptic disturbances. We clarified the regional difference of the relation among dust outbreak, surface wind, and land surface condition by analyzing the correlation between dust outbreak frequency and strong wind frequency when the threshold velocity is set to be a constant, 6.5 m/sec. From this analysis, we found that the surface wind primarily controls dust outbreaks in desert regions in March and April. On the other hand, land surface conditions primarily control dust outbreaks in Grassland. When we consider the effect of snow cover, remarkable effects of snow cover are found in Inner Mongolia and Hexi Corridor in March, and Northern Mongolia in April.
机译:利用1988年3月至2004年5月的地面气象资料,对东亚沙尘事件特征的地区差异进行了研究。根据地形和土地覆盖类型,东亚被分为11个地区。在这些地区中,粉尘暴发经常发生在戈壁沙漠,黄土高原西部和塔克拉玛干沙漠中,其土地覆盖类型为裸露沙漠和半沙漠灌木(即沙漠)。尽管在这些区域中经常发生粉尘暴发的结果,但浮尘的频率却相差很大。在塔克拉玛干沙漠中经常观察到浮尘。另一方面,在戈壁沙漠和黄土高原很少观察到浮尘。在这些地区,尽管天气干扰产生了粉尘,但这些天气干扰立即将其清除。通过分析将阈值速度设为恒定值6.5 m / sec时尘埃爆发频率与强风频率之间的相关性,阐明了尘埃爆发,地表风和陆地表面状况之间关系的区域差异。通过此分析,我们发现地面风主要控制3月和4月沙漠地区的粉尘暴发。另一方面,地表条件主要控制了草原的粉尘暴发。当我们考虑积雪的影响时,在内蒙古和河西走廊的三月和四月的蒙古北部发现了积雪的显着效果。

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